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Wetland oxygen How do coastal wetlands breathe in waterlogged soils?

Trace oxygen gradients, roots, microbes, sulfide, methane, carbon, and field evidence through the hidden chemistry of coastal wetlands.

5
lessons
~20 min
to learn
🔬 Science
subject
Adults
level
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What you’ll learn

  1. Water blocks airExplain how saturation, flooding, and diffusion create oxygen gradients in wetland soils.Water-filled pores slow oxygen movement and create changing zones from the surface to deeper sediment.
  2. Plants move oxygenDescribe how wetland roots, aerenchyma, mangrove structures, and burrows change local oxygen conditions.Plants and animals create narrow pathways that help them cope with oxygen-poor sediment.
  3. Microbes change chemistryConnect redox conditions with alternative microbial pathways and transformations of sulfur, iron, nitrogen, and carbon.Microbes continue decomposition without oxygen, changing the compounds and gases found in wetland soils.
  4. Animals and carbonRelate burrowing, salinity, decomposition, methane, and tidal export to wetland carbon budgets.Animals and microbes connect hidden soil chemistry with habitat structure and carbon storage or release.
  5. Measure and manageUse field, chemical, and landscape evidence to interpret wetland oxygen conditions and guide adaptive management.Good decisions pair surface maps with repeated measurements of the processes below the waterline.

Questions this course answers

Why does saturation usually reduce oxygen movement through soil?

Water-filled pores replace air pathways, and oxygen moves much more slowly through water.

What can create a small oxygenated patch below the surface?

Roots and burrows can create narrow pathways that bring oxygen into otherwise reducing sediment.

Put the root-oxygen pathway in a simple order.

Aerenchyma can connect exposed tissues with roots, allowing gases to affect the surrounding rhizosphere.

What is a pneumatophore?

Pneumatophores rise above saturated sediment and provide part of a mangrove plant's gas-exchange system.

What can microbes use when oxygen is scarce?

Anaerobic microbes can use several alternative acceptors while breaking down organic matter.

Why can coastal wetland mud smell like rotten eggs?

Sulfate reduction in oxygen-poor coastal sediment can produce sulfide, a compound associated with that smell.

Grounded in trusted sources

  • U.S. Environmental Protection Agency, What is a Wetland?, https://www.epa.gov/wetlands/what-wetland
  • NOAA Ocean Service, What is a salt marsh?, https://oceanservice.noaa.gov/facts/saltmarsh.html
  • NOAA Ocean Service, Coastal Blue Carbon, https://oceanservice.noaa.gov/ecosystems/coastal-blue-carbon/
  • U.S. Environmental Protection Agency, Nutrient Criteria Technical Guidance Manual: Wetlands, https://nepis.epa.gov/Exe/ZyPURL.cgi?Dockey=P1009KCU.TXT
  • U.S. Geological Survey, Getting to the root of plant-mediated methane emissions and oxidation in a thermokarst bog, https://www.usgs.gov/publications/getting-root-plant-mediated-methane-emissions-and-oxidation-a-thermokarst-bog
  • NOAA Ocean Service, Monitoring Estuaries: Dissolved Oxygen, https://oceanservice.noaa.gov/education/tutorial_estuaries/est10_monitor.html

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